James J. Wray¹, Sarah T. Hansen¹, Josef Dufek¹, Gregg A. Swayze², Scott L. Murchie³, Frank P. Seelos³, John R. Skok⁴, Rossman P. Irwin III⁵ and Mark S. Ghiorso⁶

¹School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia 30332, USA
²US Geological Survey, Denver, Colorado 80225, USA
³Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland 20723, USA
⁴Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana 70803, USA
⁵Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Washington DC 20013, USA
⁶OFM Research, Seattle, Washington 98115, USA

We still seek a copyright agreement with Nature to display abstracts of their cosmochemistry related publications.

Reference
Wray JJ, Hansen ST, Dufek J, Swayze GA, Murchie SL, Seelos FP, Skok JR, Irwin III RP and Ghiorso MS (2013) Prolonged magmatic activity on Mars inferred from the detection of felsic rocks. Nature Geoscience 6:1013–1017.
[doi:10.1038/ngeo1994]

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